Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Journal Paper

Paper Information

مرکز اطلاعات علمی Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Verion

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

video

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

sound

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Persian Version

Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

View:

498
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Download:

0
Scientific Information Database (SID) - Trusted Source for Research and Academic Resources

Cites:

Information Journal Paper

Title

Petrogenesis of Neogene dacitic and andesitic volcanism in the Tel Gorban-Chah Breshk area North of Shahrebabak, Kerman-Iran

Pages

  11-22

Abstract

Neogene volcanism in the Tel Gorban-Chah Breshk area, north of Shahre-Babak, occurs as dacitic to andesitic lava flows and domes. Petrographically the rocks consist of plagioclase, hornblende ± biotite and quartz phenocrysts setting in porphyritic and hyalopilitic matrix. Opacitization of hornblende and biotite and zoning and sieve texture in plagioclase are signatures of disequilibrium conditions through the magma cooling. Geochemical data and petrological diagrams show their medium potassic calc-alkaline nature. Enrichment in LILE’ s and depletion in HFSE’ s (eg. Nb, Ta, Ti) points to a subduction tectonic environment for Tel Gorban-Chah Breshk dacitic to andesitic rocks. Furthermore, their Al2O3>16, Sr/Y>80 and chondrite normalize REE pattern are quite similar to dakites. Distinctive geochemical features such as Rb/Sr< 0. 04, La/Yb> 18, Yb< 1, (Sr/Y)n> 80, and Y<10, suggest their derivation from partial melting of a subducted oceanic lithosphere with the garnet remains in the source region. They are emplaced along the faults and fractures in the post collisional tectonic regime in the Neogene time.

Cites

  • No record.
  • References

  • No record.
  • Cite

    APA: Copy

    HOSSEINI, S.Z., & ARVIN, M.. (2016). Petrogenesis of Neogene dacitic and andesitic volcanism in the Tel Gorban-Chah Breshk area North of Shahrebabak, Kerman-Iran. GEOSCIENCES, 26(101 ), 11-22. SID. https://sid.ir/paper/31828/en

    Vancouver: Copy

    HOSSEINI S.Z., ARVIN M.. Petrogenesis of Neogene dacitic and andesitic volcanism in the Tel Gorban-Chah Breshk area North of Shahrebabak, Kerman-Iran. GEOSCIENCES[Internet]. 2016;26(101 ):11-22. Available from: https://sid.ir/paper/31828/en

    IEEE: Copy

    S.Z. HOSSEINI, and M. ARVIN, “Petrogenesis of Neogene dacitic and andesitic volcanism in the Tel Gorban-Chah Breshk area North of Shahrebabak, Kerman-Iran,” GEOSCIENCES, vol. 26, no. 101 , pp. 11–22, 2016, [Online]. Available: https://sid.ir/paper/31828/en

    Related Journal Papers

    Related Seminar Papers

  • No record.
  • Related Plans

  • No record.
  • Recommended Workshops






    Move to top